Subsidence in Maceio, Brazil, Characterized by Dinsar and Inverse Modeling

P. Euillades, L. Euillades, P. Rosell, Y. Roa
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引用次数: 4

Abstract

The city of Maceió has been historically affected by cracks and sink events in buildings and city infrastructure. Availability of a consistent Sentinel 1 Mission dataset between 2014 and 2019 allows characterizing the undergoing crustal deformation process that provokes such effects. We processed a dataset of 81 SAR scenes using the DInSAR-SBAS time-series technique, which allowed us to obtain mean velocity of deformation and deformation time series. Detected displacement patterns show subsidence concentrated in the Mundaú lagoon coast in front of Mutange, Pinheiro and Levada neighbourhoods. Inversion of the results, using analytical models, locates a sill-like source at ~400m depth and with a radius of ~0.8 km. Its depth would be compatible with re-activation of the Mutange fault system, possibly related to salt mining operations in the area. Further investigation is needed to better constrain the deformation source and to identify if the observed process was active before the analysed time span.
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基于Dinsar和反演模型的巴西Maceio地区沉陷特征
历史上,Maceió市一直受到建筑物和城市基础设施裂缝和下沉事件的影响。哨兵1号任务在2014年至2019年之间的一致数据集的可用性可以表征引发这种效应的正在发生的地壳变形过程。我们使用DInSAR-SBAS时间序列技术处理了81个SAR场景的数据集,该技术使我们能够获得平均变形速度和变形时间序列。检测到的位移模式显示沉降集中在Mutange、Pinheiro和Levada社区前面的Mundaú泻湖海岸。利用解析模型对结果进行反演,确定了一个井状震源,震源深度约400米,半径约0.8 km。它的深度将与Mutange断层系统的重新激活相适应,这可能与该地区的盐矿开采作业有关。需要进一步的研究来更好地约束变形源,并确定观察到的过程是否在分析的时间跨度之前是活跃的。
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